47 citations as recorded by crossref.

1. Andic Soil Properties and Tephra Layers Hamper C Turnover in Icelandic Peatlands S. Möckel et al. 10.1029/2021JG006433
2. Aged soils contribute little to contemporary carbon cycling downstream of thawing permafrost peatlands A. Tanentzap et al. 10.1111/gcb.15756
3. Drained organic soils under agriculture — The more degraded the soil the higher the specific basal respiration A. Säurich et al. 10.1016/j.geoderma.2019.113911
4. Estimation of sulfur fate and contribution to VSC emissions from lakes during algae decay J. Wang et al. 10.1016/j.scitotenv.2022.159193
5. Soil Quality and Organic Matter Pools in a Temperate Climate (Northern Italy) under Different Land Uses L. Vittori Antisari et al. 10.3390/agronomy11091815
6. Variation of δ15N in Indian coal, lignite and peat M. Ganguly et al. 10.1016/j.chemer.2023.126013
7. High methane emissions from thermokarst lakes in subarctic peatlands A. Matveev et al. 10.1002/lno.10311
8. Stable carbon isotopic composition of peat columns, subsoil and vegetation on natural and forestry-drained boreal peatlands H. Nykänen et al. 10.1080/10256016.2018.1523158
9. Mineral protection controls soil organic carbon stability in permafrost wetlands Y. Wang et al. 10.1016/j.scitotenv.2023.161864
10. From fibrous plant residues to mineral-associated organic carbon – the fate of organic matter in Arctic permafrost soils I. Prater et al. 10.5194/bg-17-3367-2020
11. Storage and drivers of soil organic carbon and nitrogen in a rangeland ecosystem across a lithosequence in western Iran M. Karimi Nezhad 10.1016/j.catena.2019.01.018
12. Soil Biochemical Indicators and Biological Fertility in Agricultural Soils: A Case Study from Northern Italy L. Vittori Antisari et al. 10.3390/min11020219
13. Rapid organic matter assay of organic matter degradation across depth gradients within marine sediments T. O'Meara et al. 10.1111/2041-210X.12894
14. Riparian wetland properties counter the effect of land-use change on soil carbon stocks after rainforest conversion to plantations N. Hennings et al. 10.1016/j.catena.2020.104941
15. Biogeochemical indicators of peatland degradation – a case study of a temperate bog in northern Germany J. Krüger et al. 10.5194/bg-12-2861-2015
16. The patchiness of soil 13C versus the uniformity of 15N distribution with geomorphic position provides evidence of erosion and accelerated organic matter turnover M. Ghotbi et al. 10.1016/j.agee.2023.108616
17. Carbon, nitrogen and their stable isotope (δ13C and δ15N) records in two peat deposits of Central Siberia: raised bog of middle taiga and palsa of forest-tundra ecotone A. Prokushkin et al. 10.1088/1755-1315/1093/1/012007
18. Stable Carbon Isotopes δ13C as a Proxy for Characterizing Carbon Sources and Processes in a Small Tropical Headwater Catchment: Nsimi, Cameroon G. Nkoue Ndondo et al. 10.1007/s10498-020-09386-8
19. Chemical Composition of Soil Organic Matter in a Subarctic Peatland: Influence of Shifting Vegetation Communities A. Normand et al. 10.2136/sssaj2016.05.0148
20. Palsa Uplift Identified by Stable Isotope Depth Profiles and Relation of δ15 N to C/N Ratio J. Krüger et al. 10.1002/ppp.1936
21. Rewetting and Drainage of Nutrient-Poor Peatlands Indicated by Specific Bacterial Membrane Fatty Acids and a Repeated Sampling of Stable Isotopes (δ15N, δ13C) M. Groß-Schmölders et al. 10.3389/fenvs.2021.730106
22. Spatial Patterns of Carbon and Nitrogen in Soils of the Barents Sea Coastal Area (Khaypudyrskaya Bay) E. Shamrikova et al. 10.1134/S1064229319030098
23. The evolution of hummock–depression micro‐topography in an alpine marshy wetland in Sanjiangyuan as inferred from vegetation and soil characteristics G. Wu et al. 10.1002/ece3.7278
24. Water Table Drawdown Alters Soil and Microbial Carbon Pool Size and Isotope Composition in Coastal Freshwater Forested Wetlands K. Minick et al. 10.3389/ffgc.2019.00007
25. Water table drawdown reshapes soil physicochemical characteristics in Zoige peatlands L. Liu et al. 10.1016/j.catena.2018.05.025
26. Switch of fungal to bacterial degradation in natural, drained and rewetted oligotrophic peatlands reflected in <i>δ</i><sup>15</sup>N and fatty acid composition M. Groß-Schmölders et al. 10.5194/soil-6-299-2020
27. Organic geochemical evidence of postglacial paleoenvironmental evolution of the Comeya peatland (Asturias, N Spain) J. Urbańczyk et al. 10.1016/j.coal.2016.10.001
28. Calculating carbon changes in peat soils drained for forestry with four different profile-based methods J. Krüger et al. 10.1016/j.foreco.2016.09.006
29. The impact of long-term water level draw-down on microbial biomass: A comparative study from two peatland sites with different nutrient status P. Mpamah et al. 10.1016/j.ejsobi.2017.04.005
30. Ground ice at depths in the Tianshuihai Lake basin on the western Qinghai-Tibet Plateau: An indication of permafrost evolution Y. Yang et al. 10.1016/j.scitotenv.2020.138966
31. Organic composition and multiphase stable isotope analysis of active, degrading and restored blanket bog L. McAnallen et al. 10.1016/j.scitotenv.2017.05.064
32. Development of permafrost-affected peatlands in the southern limit of the European Russian cryolithozone and their vulnerability to future warming A. Pastukhov et al. 10.1016/j.scitotenv.2022.154350
33. Carbon‑sulfur coupling in a seasonally hypoxic, high-sulfate reservoir in SW China: Evidence from stable C S isotopes and sulfate-reducing bacteria M. Yang et al. 10.1016/j.scitotenv.2022.154537
34. Effects of peat decomposition on δ13C and δ15N depth profiles of Alpine bogs S. Drollinger et al. 10.1016/j.catena.2019.02.027
35. Peat decomposition proxies of Alpine bogs along a degradation gradient S. Drollinger et al. 10.1016/j.geoderma.2020.114331
36. Stable isotopes (δ13C, δ15N) and biomarkers as indicators of the hydrological regime of fens in a European east–west transect M. Groß-Schmölders et al. 10.1016/j.scitotenv.2022.156603
37. Comparison of plant litter and peat decomposition changes with permafrost thaw in a subarctic peatland Z. Wang & N. Roulet 10.1007/s11104-017-3252-7
38. Formation processes of shallow ground ice in permafrost in the Northeastern Qinghai-Tibet Plateau: A stable isotope perspective Y. Yang et al. 10.1016/j.scitotenv.2022.160967
39. Dissolved Organic Carbon (DOC) in Ground Ice on Northeastern Tibetan Plateau Y. Yang et al. 10.3389/feart.2022.782013
40. Depth profiles of soil organic carbon isotopes across a lithosequence: implications for drivers of soil δ13C vertical changes M. Karimi Nezhad et al. 10.1080/10256016.2022.2044806
41. Biochemical components of Sphagnum and persistence in peat soil G. Pipes & J. Yavitt 10.1139/cjss-2021-0137
42. Influence of vegetation cover and soil features on CO2, CH4 and N2O fluxes in northern Finnish Lapland A. Lagomarsino & A. Agnelli 10.1016/j.polar.2020.100531
43. Vascular plants affect properties and decomposition of moss-dominated peat, particularly at elevated temperatures L. Zeh et al. 10.5194/bg-17-4797-2020
44. Substrate quality of drained organic soils—Implications for carbon dioxide fluxes A. Säurich et al. 10.1002/jpln.202000475
45. Markers of Soil Organic Matter Transformation in Permafrost Peat Mounds of Northeastern Europe A. Pastukhov et al. 10.1134/S1064229318010131
46. Carbon storage change and δ13C transitions of peat columns in a partially forestry-drained boreal bog H. Nykänen et al. 10.1007/s11104-019-04375-5
47. Impacts of donor-peat management practices on the functional characteristics of a constructed fen F. Nwaishi et al. 10.1016/j.ecoleng.2015.04.038